Around 550 million years ago, the Earth was in the late Ediacaran period, which is part of the Neoproterozoic era. This period is characterized by the appearance of the first complex multicellular life forms, including the Ediacaran biota, which consisted of soft-bodied organisms. This era set the stage for the Cambrian explosion, which followed shortly after, leading to a rapid diversification of life. The late Ediacaran is crucial for understanding the evolution of early life on Earth.
It is a term from Geology, is an interval of geological time from about 250 million years ago to about 65 million years ago.
It is a geological site, formed as of the result of volcanic activity over 50 million years ago. It is also a World Heritage Site.It is a geological site, formed as of the result of volcanic activity over 50 million years ago. It is also a World Heritage Site.It is a geological site, formed as of the result of volcanic activity over 50 million years ago. It is also a World Heritage Site.It is a geological site, formed as of the result of volcanic activity over 50 million years ago. It is also a World Heritage Site.It is a geological site, formed as of the result of volcanic activity over 50 million years ago. It is also a World Heritage Site.It is a geological site, formed as of the result of volcanic activity over 50 million years ago. It is also a World Heritage Site.It is a geological site, formed as of the result of volcanic activity over 50 million years ago. It is also a World Heritage Site.It is a geological site, formed as of the result of volcanic activity over 50 million years ago. It is also a World Heritage Site.It is a geological site, formed as of the result of volcanic activity over 50 million years ago. It is also a World Heritage Site.It is a geological site, formed as of the result of volcanic activity over 50 million years ago. It is also a World Heritage Site.It is a geological site, formed as of the result of volcanic activity over 50 million years ago. It is also a World Heritage Site.
No. The Cambrian period was abut 550 million years ago, the earliest humans existed only 200,000 years ago
The Quaternary Period (from 2.59 Million years ago to the present day).
The planet Earth is about 4,600 million years old. Fossil evidence becomes abundant in the geological record in the Cambrian Era, which was about 550 million years ago (when hard shelled animals appeared) Therefore (550/4600)*100 = roughly 12% of Geological time contains abundant fossil evidence. However, please note that (non abundant) fossil evidence goes back about 3600 million years, (3600/4600)*100 = roughly 73% of Geologic time.
It is on the coast of Northern Ireland and it is a geological formation from volcanic activity about 50 to 60 million years ago.It is on the coast of Northern Ireland and it is a geological formation from volcanic activity about 50 to 60 million years ago.It is on the coast of Northern Ireland and it is a geological formation from volcanic activity about 50 to 60 million years ago.It is on the coast of Northern Ireland and it is a geological formation from volcanic activity about 50 to 60 million years ago.It is on the coast of Northern Ireland and it is a geological formation from volcanic activity about 50 to 60 million years ago.It is on the coast of Northern Ireland and it is a geological formation from volcanic activity about 50 to 60 million years ago.It is on the coast of Northern Ireland and it is a geological formation from volcanic activity about 50 to 60 million years ago.It is on the coast of Northern Ireland and it is a geological formation from volcanic activity about 50 to 60 million years ago.It is on the coast of Northern Ireland and it is a geological formation from volcanic activity about 50 to 60 million years ago.It is on the coast of Northern Ireland and it is a geological formation from volcanic activity about 50 to 60 million years ago.It is on the coast of Northern Ireland and it is a geological formation from volcanic activity about 50 to 60 million years ago.
Geological conditions created the Matterhorn commencing some 200 million years ago. The shape as we know it today comes from a million years of erosion
The Matterhorn was created through geological conditions commencing some 200 million years ago. The modern shape is caused by a million years of erosion
The Paleozoic Era lasted from about 540 million years ago to about 280 million years ago. It included the Cambrian, Ordovician, Silurian, Devonian, Carboniferous, and Permian Periods.
About 90 million years ago, New Zealand started to leave the Gondwana landmass, and was quite separate by 50 million years ago. The Tasman Sea had by then stopped spreading. Some of the older rocks (about 550 million years ago) were formed when it was still part of Gondwana.
4600 million years ago would be around the time of the Hadean Eon, a period in Earth's history known for its intense heat and heavy bombardment by asteroids and comets. This was a time when the Earth was still forming and undergoing significant geological and environmental changes.
The Cenozoic, which began 65 million years ago, and includes the present times.